{"id":132742,"date":"2018-03-11T12:58:48","date_gmt":"2018-03-11T12:58:48","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-glaciarismo-cuaternario-en-el-alto-aragon-occidental\/"},"modified":"2018-03-11T12:58:48","modified_gmt":"2018-03-11T12:58:48","slug":"el-glaciarismo-cuaternario-en-el-alto-aragon-occidental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-glaciarismo-cuaternario-en-el-alto-aragon-occidental\/","title":{"rendered":"El glaciarismo cuaternario en el alto aragon occidental."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Carlos Enrique Marti Bono <\/strong><\/h2>\n<p>Se estudian los dep\u00f3sitos glaciares, fluvioglaciares y glaciolacustres de los valles de los r\u00edos veral, arag\u00f3n subord\u00e1n, osia, estarr\u00fan, arag\u00f3n, aur\u00edn y g\u00e1llego, asi como las formas de relieve (circos y valles) relacionadas con el fen\u00f3meno glaciar.  tambi\u00e9n se dedica un cap\u00edtulo a formas y dep\u00f3sitos periglaciares correspondientes a la \u00faltima glaciaci\u00f3n y a los actualmente a\u00fan funcionales.  se identifican 206 circos glaciares, cuyas dimensiones, altitud y litolog\u00eda se estudian estad\u00edsticamente. Dichos circos eran el origen de lenguas glaciares que terminaban a 800-900 m. De altitud en los valles del g\u00e1llego y del arag\u00f3n y entre 950 y 1130 m. En los dem\u00e1s valles, con un nivel de equilibrio glaciar cercano a 1700 m. Durante la fase de m\u00e1ximo.  los glaciares de valle dieron lugar a lagos de obturaci\u00f3n, de los que se han identificado 16 y estudiado sus dep\u00f3sitos.  las acaracter\u00edsticas de las terrazas fluvioglaciares permiten definir la existencia de dos grandes periodos glaciares; los dep\u00f3sitos del pen\u00faltimo son escasos y se localizan en el valle del g\u00e1llego.  en todos los valles destaca la ausencia de grandes cubetas de sobreexcavaci\u00f3n, a diferencia de lo que ocurre en el pirineo central.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El glaciarismo cuaternario en el alto aragon occidental.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El glaciarismo cuaternario en el alto aragon occidental. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Carlos Enrique Marti Bono <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 13\/12\/1996<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n<h3>Direcci\u00f3n y tribunal<\/h3>\n<ul>\n<li><strong>Director de la tesis<\/strong>\n<ul>\n<li>Oriol Riba Arderiu<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: david Serrat congost <\/li>\n<li>mateo Guti\u00e9rrez elorza (vocal)<\/li>\n<li>Antonio Gomez ortiz (vocal)<\/li>\n<li>Jos\u00e9 m. Garcia   ruiz (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Carlos Enrique Marti Bono Se estudian los dep\u00f3sitos glaciares, fluvioglaciares y glaciolacustres de los valles de los [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"var(--ast-global-color-4)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[951,27,953,445,75],"tags":[19924,246642,446,246643,7599,80],"class_list":["post-132742","post","type-post","status-publish","format-standard","hentry","category-barcelona","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-glacial","category-geomorfologia","tag-antonio-gomez-ortiz","tag-carlos-enrique-marti-bono","tag-david-serrat-congost","tag-jose-m-garcia-ruiz","tag-mateo-gutierrez-elorza","tag-oriol-riba-arderiu"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/132742","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=132742"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/132742\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=132742"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=132742"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=132742"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}